Dear all,
I would greatly appreciate references to studies on the first garnet
growth in (possibly monometamorphic) low-grade pelites, especially
cases where the stabilization of garnet by extra components, or
decreased H2O activity, lower the temperature of the Grt-in isograd.
If you reply directly to me I'll then share the references through the
mailing lists.
Have a nice weekend,
Bernardo Cesare
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